The Sub-Trenton Formations of Indiana

Total Page:16

File Type:pdf, Size:1020Kb

The Sub-Trenton Formations of Indiana Sub-Trenton Formations 75 THE SUB-TRENTON FORMATIONS OF INDIANA. W. N. Logan, Indiana University Our knowledge of the geological formations in Indiana which are older than the uppermost part of the so-called Trenton limestone is derived solely from the study of drillings from deep wells. Deep well drilling in the search for natural gas began in Indiana about the year 1886. Within the succeeding decade a large number of wells had been drilled in many parts of the state. However, none of the earlier wells penetrated below the base of the Ordovician, in fact none of them reached the base of the Ordovician. One of the deepest of the early wells was drilled in the southwest corner of the court house square at Bloomington. This well had a depth of 2,730 feet and was completed in the Shakopee limestone at a point some 400 feet above the base of the Ordovician. Attempts were made to correlate the formations encountered in the deeper wells but in the light of more recent studies some errors of correlation resulted. For instance the St. Peter sandstone of the Or- dovician was correlated with the Potsdam sandstone of the Cambrian. Interpretations and earlier correlations were based largely upon the records furnished by well drillers, and very little study of drillings was undertaken. Very naturally drillers made errors in interpretation which led to errors of correlation. In recent years drillings from many deep wells have been obtained and these have been studied in the laboratory to the end that we are now able to correlate with greater confidence. The deepest well in Indiana was drilled at Greentown in Howard County. This well was drilled by the Chicago Gas Company. It lacks only four feet of being 4,000 feet in depth. Through the courtesy of that company the writer has obtained a remarkably complete set of drillings from this well. The samples taken were for each five feet of depth. A study of these samples and the samples from other deep wells in Indiana has enabled the writer to make the following correlations of the Sub-Trenton formations of the state. The most complete section was obtained from the Greentown well and that section is referred to in the succeeding pages as the type section. The Ordovician Period. The St. Peter Sandstone.—The formation immediately underlying the Trenton limestone in Indiana is the St. Peter sandstone which be- longs to the Canadian division of the Ordovician. The sandstone is com- posed of small rounded grains of translucent to transparent quartz which are cemented with a calcareous or dolomitic cement. The size of the grains of the St. Peter sandstone at its outcrop at Ottawa, Illinois, varies from .1 mm to 1 mm in diameter, the average being about .5 mm. "Proc. Ind. Acad. Sci., vol. 34, 1924 (1925)." 76 Proceedings of Indiana Academy of Science The grains from the Indiana wells are much smaller, ranging from .01 mm to .2 mm in diameter. Among the quartz grains are many par- ticles of pyrite. Where these particles have been oxidized the quartz grains are stained yellow though the sandstone is commonly white. The thickness of the St. Peter in Indiana varies from 15 feet to more than 200 feet. It appears to have a minimum thickness near the apex of the Cincinnati geanticline and to increase in thickness in the basins beyond the arch. There is apparently an increase in fineness of grain from bottom to top. At East Chicago the St. Peter has a thickness of 75 feet; at Green- town, 120 feet; at Cloverdale, 70 feet; at Bloomington, 224 feet; at Greensburg, 188 feet; and at Middlefork, 210 feet. The Shakopee Limestone.—The formation which underlies the St. Peter sandstone in Indiana is a white to yellowish-gray, cherty, dolomitic limestone which the writer has assigned to the Shakopee formation of the Canadian division of the Ordovician. While the formation is largely limestone there are layers of sand- stone and thin beds of chert present. Near the middle of the formation there are some layers of sandstone which are fine of grain and resemble the St. Peter in texture and appearance. The thickness of the Shakopee in Indiana varies from 72 to 100 feet, usually, though at East Chicago the formation is credited with a thickness of 314 feet. In the Greentown well the thickness is 80 feet; in the Lacrosse well, 95 feet; in the Clover- dale well, 72 feet; and in the Greensburg well, 100 feet. The New Richmond Sandstone.—A calcareous sandstone lies be- neath the Shakopee limestone. This formation is correlated with the New Richmond which is the basal member of the Canadian division of the Ordovician. The drillings from the formation consist of rounded quartz grains of white, yellow or brown color. They also contain pyrite crystals and white and yellow calcareous particles and a few chert particles. The thickness of the New Richmond in Indiana varies from 26 to 210 feet. In the Cloverdale well the thickness assigned to it is 210 feet; in the Greentown well, 180 feet; in the Middle Fork well, 45 feet; in the East Chicago well, 26 feet. The Oneonta Dolomite.—A coarse cherty limestone which underlies the New Richmond sandstone has been correlated with the Oneonta dolo- mite, which may be Cambrian. The driRings of this formation are com- posed of coarse particles of limestone and chert which are white or yellow in color. Pyrite crystals are present and many of the grains are stained with limonite. This formation is placed by Ulrich and Walcott in the Ozarkian division of geologic time. In Wisconsin the formation has a thickness varying from 100 to 200 feet. In Indiana the thickness varies from 67 to 105 feet. In the Greentown well the assigned thickness is 100 feet; in the Cloverdale well, 67 feet; in the Lacrosse well, 70 feet; in the Greensburg well, 94 feet; and in the East Chicago well, 105 feet. Sub-Trenton Formations 77 The Madison Sandstone.—Drillings from the Greentown well show a fine grained calcareous sandstone lying beneath the Oneonta dolomite. This formation has been assigned to the Madison formation. The thick- ness of the sandstone is 30 feet which is the thickness it attains in eastern Wisconsin. In the other deep wells of the state the Madison is not differentiated but it is probably included in the Oneonta. The Mendota Dolomite.—A fine sandy dolomitic limestone lies be- neath the Madison sandstone in the Greentown well. This formation has been assigned to the Mendota. Its thickness is 25 feet and in eastern Wisconsin it has a thickness of 20 feet. In the other deep wells of In- diana, the formation has not been differentiated and probably is included with an adjacent formation. The Mendota is included in the Ozarkian. The Devil's Lake Sandstone.—In the Greentown well the drillings reveal the presence of a white fine-grained sandstone beneath the Men- dota dolomite. This formation has been assigned to the Devil's Lake horizon of the Ozarkian. The drillings consist of fine quartz grains, some broken fragments of larger quartz grains, some pyrite concretions, and calcareous matter. The thickness of the sandstone in the Greentown well is 100 feet and it has about the same thickness in eastern Wisconsin. This formation is assumed by the writer to be the basal member of the Ozarkian in northern Indiana. The Cambrian Period. The Jordan Sandstone.—Below the Devil's Lake sandstone is a sandstone composed of larger grains which are stained red or grayish- brown in color. This formation contains much more pyrite than the overlying sandstone. It has been assigned to the Jordan formation of the Cambrian. It has a thickness of 150 feet in the Greentown well. As differentiated in the Cloverdale well it has a thickness of 223 feet; in the Greensburg well 200 feet ; and in the Bryant well, 60 feet. In the latter some of the rocks above may belong to the Jordan horizon. The formation in the Bryant well contains fresh water. The Jordan is the source of fresh water supplies in the Chicago region. The Lodi Shale.—In the Greentown well the Jordan sandstone rests upon a bed of shale which has a thickness of 45 feet. This shale is probably equivalent to the Lodi shale in the Wisconsin section of Ulrich. In his Wisconsin section Ulrich suggests the Thempealeau Epoch to in- clude the Norwalk sandstone, the Lodi shale member, the St. Lawrence limestone and a basal shale (unnamed). The Norwalk sandstone is absent in eastern Wisconsin and appears to be absent in Indiana. At least the writer was not able to differentiate the horizon. The Lodi shale has a thickness of 50 feet in western Wisconsin and a maximum thick- ness of 25 feet in eastern Wisconsin. The St. Lawrence Limestone.—Beneath the Lodi shale is a shaly dolomitic limestone which has a thickness of 45 feet in the Greentown well. The St. Lawrence has been used by some writers to include more than the limestone stratum. The basal shale layer which is present in 78 Proceedings of Indiana Academy of Science the Wisconsin section seems to be absent in Indiana. In the Iowa sec- tion the St. Lawrence is represented by 50 feet of sandy dolomitic lime- stone, which corresponds very closely with the thickness in the Green- town well. The Franconia Sandstone.—A series of glauconitic sandstones con- taining thin beds of shale and shaly limestone lie below the St. Law- rence limestone in Indiana. Three divisions are recognizable.
Recommended publications
  • A Hydrogeologic and Mapping Investigation of the St. Lawrence Formation in the Twin Cities Metropolitan Area Executive Summary T
    Minnesota Geological Survey (MGS) Open File Report 06-04 (Open File Reports are not subjected to conventional MGS editorial standards) A HYDROGEOLOGIC AND MAPPING INVESTIGATION OF THE ST. LAWRENCE FORMATION IN THE TWIN CITIES METROPOLITAN AREA Runkel, A.C., Mossler, J.H., Tipping, R.G., and Bauer, E.J. Minnesota Geological Survey 2642 University Ave W., St. Paul, Minnesota 55114-1057 EXECUTIVE SUMMARY This report summarizes the results of a two year project conducted by the Minnesota Geological Survey to map the Upper Cambrian St. Lawrence Formation and investigate its hydrologic properties in the Twin Cities Metropolitan area (TCMA). Funding was provided by the Minnesota Department of Health. Final products are a map delivered in electronic format that can be used with Arcview 3.2 GIS software, and this informal report. Our hydrogeologic study indicates that the St. Lawrence Formation commonly has a moderate to high horizontal hydraulic conductivity across all of the study area. In conditions of shallow burial beneath younger bedrock it is most similar in the development of secondary pores and measured hydraulic properties to fractured carbonate rock aquifers. Discrete intervals with secondary pores have a high horizontal hydraulic conductivity whereas rock between these intervals are orders of magnitude lower in conductivity. The properties of the St. Lawrence Formation in a vertical direction are not as well- understood, but available data are consistent with the traditional classification of the formation as an aquitard. However, the integrity of the formation as an aquitard in a vertical direction, particularly under conditions of shallow burial such as where it is uppermost bedrock, has not been rigorously tested, and may be markedly variable across the TCMA.
    [Show full text]
  • Geologic Atlas of Blue Earth County, Minnesota
    Prepared and Published with the Support of COUNTY ATLAS SERIES THE BLUE EARTH COUNTY BOARD OF COMMISSIONERS AND ATLAS C-26, PART A MINNESOTA GEOLOGICAL SURVEY the Minnesota ENVironment and Natural Resources Trust Fund Blue Earth County Harvey Thorleifson, Director as recommended by the LEGislatiVE-CitiZen Commission on Minnesota Resources Plate 2—Bedrock Geology NIC OLL ET COU NTY 7 Minnesota B BEDROCK GEOLOGY Ka 44°15' N. 285 300 R. 29 W. Kd m STRATIGRAPHIC COLUMN River 285 By 240 s 94° W. e i Lithostratigraphic r Composite natural gamma log 255 NICOLLET LE SUEUR COUNTY R. 26 W. COUNTY R. 25 W. e unit S 270 - e 315 Increasing count 330 Era m Lithology Kd e T. 109 N. sl Os 315 Julia R. Steenberg t Group, 0 100 s 24 Map symbol 19 y 300 300 24 24 Formation 270 lr 19 S API-G units Oo Thickness (in feet) 300 River 285 LIME JAMESTOWN 345 94°15' W. 255 Kd Wita Kd Creek 315 2012 315 )68 j Kd Lake j Dakota Kd 5-90 m.y.) Upper Formation Os Y 300 (99.6-93.5 T Duck Cretaceous 300 lr Morgan Os Lake N T. 109 N. CAMBRIA U 315 O 300 Minnesota 240 Ballantyne C LOCATION DIAGRAM Oo 300 Lake R 270 Madison MESOZOIC R. 28 W. U 31 Kd 300 31 Oo Unnamed Ka Os E Kd 30-90 36 31 Eagle Lake lr lr 36 315 36 U 36 S Cretaceous 300 ) 31 300 22 (112-93.5 m.y.) (112-93.5 Gilfillin 315 E Lower to Upper Lake L Judson Lake 315 300 lr 240 1 6 Y 6 240 Os Platteville Formation 255 315 T Opg 6 Madison 5-20 1 1 N 6 Glenwood Formation Ph 1 255 U sl 255 1 CORRELATION OF MAP UNITS O )60 Upper 315 315 C Lake A j (450 m.y.) 315 C ? E Kd Upper Cretaceous 285 14 Kd S Lithology Key 315 A St.
    [Show full text]
  • Hydrogeology and Stratigraphy of the Dakota Formation in Northwest Iowa
    WATER SUPPLY HYDROGEOLOGY AND J.A. MUNTER BULLETIN G.A. LUDVIGSON NUMBER 13 STRATIGRAPHY OF THE B.J. BUNKER 1983 DAKOTA FORMATION IN NORTHWEST IOWA Iowa Geological Survey Donald L. Koch State Geologist and Director 123 North Capitol Street Iowa City, Iowa 52242 IOWA GEOLOGICAL SURVEY WATER-SUPPLY BULLETIN NO. 13 1983 HYDROGEOLOGY AND STRATIGRAPHY OF THE DAKOTA FORMATION IN NORTHWEST IOWA J. A. Munter G. A. Ludvigson B. J. Bunker Iowa Geological Survey Iowa Geological Survey Donald L. Koch Director and State Geologist 123 North Capitol Street Iowa City, Iowa 52242 Foreword An assessment of the quantity and quality of water available from the Dakota (Sandstone) Formation 1n northwest Iowa is presented in this report. The as sessment was undertaken to provide quantitative information on the hydrology of the Dakota aquifer system to the Iowa Natural Resources Council for alloca tion of water for irrigation, largely as a consequence of the 1976-77 drought. Most area wells for domestic, livestock, and irrigation purposes only partial ly penetrated the Dakota Formation. Consequently, the long-term effects of significant increases in water withdrawals could not be assessed on the basis of existing wells. Acquisition of new data was based upon a drilling program designed to penetrate the entire sequence of Dakota sediments at key loca tions, after a thorough inventory and analysis of existing data. Definition of the distribution, thickness, and lateral and vertical changes in composition of the Dakota Formation has permitted the recognition of two mem bers. Additionally, Identification of the rock units that underlie the Dakota Formation has contributed greatly to our knowledge of the regional geology of northwest Iowa and the upper midwest.
    [Show full text]
  • Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica
    Cement in Cambrian Sandstone : Assessing the Potential for the Generation of Respirable Silica J. Brian Mahoney Kent M. Syverson Department of Geology University of Wisconsin-Eau Claire • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter Mt. Simon Formation Eau Claire Eau Claire/Wonewoc Formation contact Tilden, WI Wonewoc/Lone Rock Formation contact Colfax, WI Jordan Formation Arcadia, WI A' A northwest Iowa southeastern west-central Minnesota Wisconsin Paleoseaward Oneota Dolomite RSL Paleolandward Jordan Ss FSL Jordan Ss St Lawrence Fm St Lawrence Fm FSL Mazom anie RSL RSL Wonewoc Ss Wonewoc Ss FSL FSL Wonewoc Ss Eau Claire Fm 100 ft 25 m Eau Claire Fm RSL Mt Simon Ss 25 miles RSL 0 40 km Fine- to coarse-grained, quartzose sandstone: nonmarine Fine- to coarse-grained, quartzose sandstone: nearshore marine Very fine grained, feldspathic sandstone, siltstone, shale: offshore siliciclas Carbonate: "offshore" subtidal and peritidal carbonate parasequence boundary or parallel to inferred parasequence boundaries unconformity correlative conformity • Geologic Setting • Industrial Silica Sand • Community Concerns • Identifying Particulate Matter Minnesota Grain Size Distribution Wisconsin Grain Size Distribution 50 50 s s e e v v e e i i S 40 s 40 n n o o ST. PETER d 30 ST. PETER d e e 30 n n i i JORDAN a JORDAN a t t e 20 e r 20 WONEWOC R WONEWOC % % MT. SIMON e e g g 10 10 a a r r e e v v A A 0 0
    [Show full text]
  • State Ge?Logical Survey
    ILLINOIS State Ge?logical Survey BULLETIN NO. 1. THE GEOLOGICAL MAP OF ILLINOIS BY STUART WELLER. URBANA: UNIVERSITY OF ILLINOIS. 1906. SPRINGFIELD: lLLI:\'OIS STATE JOURNAL Co., STATE PRINTBRs· 1 9 0 6 ., STATE GEOLOGICAL COMMISSION GOVERNOR C. S. DENEEN, Chairman, PROFESSOR T. C. CHAMBERLIN, V·ice-Oha·irman. PRESIDENT EDMUND J. JAMES Secretary. H. FOSTER BAIN, Director. ·1 CONTENTS. PAGE. Letter of transmittal.... .. .. .. ..... ..... ...... .. ... ......... .. .. .... Introduction .................................................................... ..... 8 Purpose of a geological map.............................. ............................... 8 Sources of material . .. .. .. .. .. .. .. .. .. .. ........ .... 8 Lines of deformation .............................. ........................ 11 Geological formations represented ................................ rn Cambrian........................ ........ ..... .. 13 Potsdam sandstone .. ...... ...................... 1:J Ordovician ............................................... ........................... ...... 14 Lower Magnesian limestone.......................... ... ........ 14 St. Peters sandstone . ... .... .... .. .. ..... ..... ...... .. ... ... H Trenton-Galena formation ............................................ ............... 1r:i Cincinnatian formation.... .. ...... .. .. .. .. ...... .. .... 16 Silurian ......... ...... .... .. .... ....... .... ............ ........ .... .. ...... .... .. .... ...... 17 N iag-aran limestone.... .. .. .. .. .. ... ........ ... 17 Devonian..............................
    [Show full text]
  • An Analysis of Multiple Trackways of Protichnites Owen, 1852, from the Potsdam Sandstone (Late Cambrian), St
    AN ANALYSIS OF MULTIPLE TRACKWAYS OF PROTICHNITES OWEN, 1852, FROM THE POTSDAM SANDSTONE (LATE CAMBRIAN), ST. LAWRENCE VALLEY, NY by Matthew E. Burton-Kelly A Bachelors Thesis Submitted to the Faculty of the Department of Geology of St. Lawrence University in partial fulfillment of the requirements for the degree of Bachelor of Science with Honors in Geology Canton, New York 2005 1 2 3 This thesis submitted by in partial fulfillment of the requirements for the degree of Bachelor of Science with Honors in Geology from St. Lawrence University is hereby approved by the Faculty Advisor under whom the work was done. Faculty Advisor Date Department Chairman Date ii 4 ACKNOWLEDGMENTS The author would like to thank Dr. J. Mark Erickson for his assistance and guidance throughout the course of this project, as well as the St. Lawrence University Geology Department, which provided research materials and covered transportation costs. Attendance at the annual meeting of the Northeastern Section of the Geological Society of America to present preliminary results was funded by the Jim Street Fund, St. Lawrence University Geology. Jim Dawson provided vital insight into the nature of these trackways. Any number of additional people provided support for the author, most notably Camille Partin, Trisha Smrecak, and Joanne Cavallerano, but thanks go out to all the members of the St. Lawrence University Geology Department and the St. Lawrence University Track and Field teams. iii 5 TABLE OF CONTENTS THESIS APPROVAL..........................................................................................................ii
    [Show full text]
  • Stratigraphic Succession in Lower Peninsula of Michigan
    STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation
    [Show full text]
  • Mechanical Properties of St. Peter Sandstone a Comparison of Field and Laboratory Results a Thesis Submitted to the Faculty of T
    MECHANICAL PROPERTIES OF ST. PETER SANDSTONE A COMPARISON OF FIELD AND LABORATORY RESULTS A THESIS SUBMITTED TO THE FACULTY OF THE GRADUATE SCHOOL OF THE UNIVERSITY OF MINNESOTA BY MICHAEL EUGENE DITTES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE DECEMBER, 2015 This thesis contains previously published material (Appendix E) in the “Journal of Geotechnical and Geoenvironmental Engineering” © 2002 ASCE. All other material © 2015 Michael E. Dittes All Rights Reserved. ACKNOWLEDGMENTS I would like to extend my thanks to those, who without their help I would not have been able to bring this project to completion. First and foremost, I thank Professor Joseph Labuz who took a chance on me, by offering me a TA-ship. Through my time in school, Joe helped me stay focused when I started to move off on tangents, offered timely advice, and over the years has become much more than my advisor. I am proud to think of him as a friend. Professors Andrew Drescher and Peter Huddleston also deserve special thanks for providing critical review of my work, and agreeing to sit on my thesis committee. To Ms. Tiffany Ralston who had an uncanny way of knowing what I needed to do, and how, before I knew myself. To Charles Nelson who helped me streamline my thesis project and helped me gain access to the Minnesota Library Archives construction site. To my fellow graduate students with whom I debated, joked and laughed, you helped me see things that I was missing. Your input was invaluable and you have my deep appreciation.
    [Show full text]
  • The Condition of Minnesota's Groundwater, 2007-2011
    The Condition of Minnesota’s Groundwater, 2007 - 2011 August 2013 Authors Sharon Kroening Mark Ferrey The MPCA is reducing printing and mailing costs by Acknowledgements using the Internet to distribute reports and information to wider audience. Visit our website for The Minnesota Pollution Control Agency thanks the more information. following individuals for their reviews of this report. MPCA reports are printed on 100% post-consumer Byron Adams, Minnesota Pollution Control Agency recycled content paper manufactured without chlorine or chlorine derivatives. Dr. Melinda Erickson, US Geological Survey John Hines, Minnesota Department of Agriculture Brennon Schaefer, Minnesota Department of Agriculture Andrew Streitz, Minnesota Pollution Control Agency Bill VanRyswyk, Minnesota Department of Agriculture Dave Wall, Minnesota Pollution Control Agency The Minnesota Pollution Control Agency also thanks the following for the long hours of sampling required for this study: David Duffey, Gerald Flom, Mark Lunda, Meghan McGinn, and Sophia Vaughan Project dollars provided by the Clean Water Fund (from the Clean Water, Land and Legacy Amendment). Minnesota Pollution Control Agency 520 Lafayette Road North | Saint Paul, MN 55155-4194 | www.pca.state.mn.us | 651-296-6300 Toll free 800-657-3864 | TTY 651-282-5332 This report is available in alternative formats upon request, and online at www.pca.state.mn.us . Document number: wq-am1-06 Contents Contents .............................................................................................................................................
    [Show full text]
  • The Geology of the New Richmond Sandstone, Prairie Du Chien Group, Southeastern Minnesota
    The Geology of the New Richmond Sandstone, Prairie du Chien Group, Southeastern Minnesota Cristina Robins Senior Integrative Exercise March 9, 2005 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree, Carleton College, Northfield, MN, USA i The Geology of the New Richmond Sandstone, Prairie du Chien Group, Southeastern Minnesota Cristina Robins Carleton College Senior Integrative Exercise March 9, 2004 Advisor: Dr. Clint Cowan, Carleton College Abstract: This study examines the New Richmond Sandstone, a relatively unknown heterolithic assemblage of sandstone, carbonate, and shale that is commonly considered part of the Shakopee formation of the Prairie du Chien group. Stratigraphic columns constructed from seven outcrops of the New Richmond in southeastern Minnesota and northeastern Iowa show that it varies between 7 m and 20 m in thickness within the study area and consists of two facies: the Prairie Island and the Root Valley. Previous studies found that the New Richmond was deposited in part through eolian action. SEM studies of individual grains did not confirm this. Keywords: New Richmond, sandstone, Shakopee, Prairie du Chien, Ordovician, stratigraphy, SEM data, Minnesota ii Table of Contents Introduction..................................................................................................................... 1 Literature Review .................................................................................................. 1 The Prairie du Chien Group .................................................................................
    [Show full text]
  • Preliminary Hydrogeologic Evaluation of the Cincinnati Arch Region For
    PRELIMINARY HYDROGEOLOGIC EVALUATION OF THE CINCINNATI ARCH REGION FOR UNDERGROUND HIGH-LEVEL RADIOACTIVE WASTE DISPOSAL, INDIANA, KENTUCKY, AND OHIO By Orville B. Lloyd, Jr., and Robert W. Davis U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 88-4098 Raleigh, North Carolina 1989 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information, Copies of this report can contact: be purchased from: Chief, Branch of Nuclear Waste Hydrology Books and Open-File Reports U.S. Geological Survey U.S. Geological Survey National Center, Mail Stop 410 Federal Center, Building 810 12201 Sunrise Valley Drive Box 25425 Reston, Virginia 22092 Denver, Colorado 80225 or District Chief U.S. Geological Survey Post Office Box 2857 Raleigh, North Carolina 27602 Telephone: (919) 856-4510 CONTENTS Page Abstract. ............................... 1 Introduction. ............................. 2 Background ............................ 2 Purpose and scope. ........................ 4 Previous investigations. ..................... 4 Acknowledgments.......................... 6 Methods of investigation. ....................... 6 Hydrogeology of the sedimentary rocks ................. 8 General geology. ......................... 8 Hydrogeologic framework. ..................... 14 Basal sandstone aquifer ................... 14 Potential confining unit. .................. 17 Distribution and source of freshwater, saline water, and brine. ........................... 19 Ground-water occurrence and
    [Show full text]
  • The Natural History of Pikes Peak State Park, Clayton County, Iowa ______
    THE NATURAL HISTORY OF PIKES PEAK STATE PARK, CLAYTON COUNTY, IOWA ___________________________________________________ edited by Raymond R. Anderson Geological Society of Iowa ______________________________________ November 4, 2000 Guidebook 70 Cover photograph: Photograph of a portion of the boardwalk trail near Bridal Veil Falls in Pikes Peak State Park. The water falls over a ledge of dolomite in the McGregor Member of the Platteville Formation that casts the dark shadow in the center of the photo. THE NATURAL HISTORY OF PIKES PEAK STATE PARK CLAYTON COUNTY, IOWA Edited by: Raymond R. Anderson and Bill J. Bunker Iowa Department Natural Resources Geological Survey Bureau Iowa City, Iowa 52242-1319 with contributions by: Kim Bogenschutz William Green John Pearson Iowa Dept. Natural Resources Office of the State Archaeologist Parks, Rec. & Preserves Division Wildlife Research Station 700 Clinton Street Building Iowa Dept. Natural Resources 1436 255th Street Iowa City IA 52242-1030 Des Moines, IA 50319 Boone, IA 50036 Richard Langel Chris Schneider Scott Carpenter Iowa Dept. Natural Resources Dept. of Geological Sciences Department of Geoscience Geological Survey Bureau Univ. of Texas at Austin The University of Iowa Iowa City, IA 52242-1319 Austin, TX 78712 Iowa City, IA 52242-1379 John Lindell Elizabeth Smith Norlene Emerson U.S. Fish & Wildlife Service Department of Geosciences Dept. of Geology & Geophysics Upper Mississippi Refuge University of Massachusetts University of Wisconsin- Madison McGregor District Office Amherst, MA 01003 Madison WI 53706 McGregor, IA 52157 Stephanie Tassier-Surine Jim Farnsworth Greg A. Ludvigson Iowa Dept. Natural Resources Parks, Rec. & Preserves Division Iowa Dept. Natural Resources Geological Survey Bureau Iowa Dept.
    [Show full text]